湖泊气候

鄱阳湖湖泊气候及其围垦后的变化

Climatic characteristics in Poyang Lake District and its change after reclamation

而叠层石沉积期湖泊气候相对湿润，可能是区域性气候循环的结果。

But it was relative wet when stromatolite deposited , possibly resulted form the regional climatic circulate .

盐湖/湖泊是气候变化的一面镜子。

Salt lakes are a mirror of climatic change .

以往对于水体的小气候效应研究多集中于观测试验，尤其是研究大面积河流、湖泊的气候效应较多。

The existing observing and analysis focus on the climatic effect of the large lake and river rather than the microclimatic effect of water area in urban .

内陆湖泊是气候变化敏感的指示器，高山湖泊处于自然状态，受人类活动影响较小，能够较真实地反映气候状况，而内陆河尾闾湖变化是自然和人类活动共同作用的结果。

Inland lakes are sensitive indicators of climate change . High mountain lakes , due to less influence from human activity , can reflect the climate state accurately .

近50a中国寒区与旱区湖泊变化的气候因素分析

Climatic Implications on Variations of Lakes in the Cold and Arid Regions of China during the Recent 50 Years

盐类沉积韵律对研究湖泊环境及气候变迁有重要意义。

Lake sedimentary rhythm provides important information on the reconstruction of the palaeo-environment and palaeo-climate .

内蒙岱海是位于东南季风区的西北边缘的内陆封闭湖泊，对气候变化十分敏感。

Daihai Lake , with a closed drainage basin , is very sensitive to the paleoclimate hange .

其他的湖泊可能因为气候的变化，或者因为流进这些湖泊的河流干枯，而慢慢地干枯。

Others may slowly dry up because of a change in climate or because the streams that feed them dry up .

为研究青藏高原的湖泊演化、气候变化、古地理变迁及其隆升过程等提供了新资料。

The study provide new data for the study of the lake evolution , climate change , paleogeographic change and the plateau uplift process .

湖泊沉积作为气候和环境变化的信息库，能提供时间分辨率高达百年至十年尺度的气候变化信息。

As the information database of climatic and environmental changes , lake sediment provides high-resolution climatic change information which at the scale of century or even decade .

虽然未来年降水总量的变幅没有超过过去50年器测记录变幅，更不及全新世的降水变化量，但湖泊水量对气候变化的反映变率较变幅要大。

Although the future changes in precipitation are equivalent to the last 50-yr gauges and lower than changes in the Holocene , the speed of lake water change was much high .

内陆干旱&半干旱气候区封闭湖泊对区域气候变化的响应十分敏感，能够提供时间分辨率高达百年甚至十年尺度的气候变化信息。

Lake sediment in arid or semi-arid areas is abundant in information of climate and environment changes , which is helpful for us to set up high-resolution environment changes sequence at the scale of decade .

而对于陆相盆地而言，由于湖泊沉积对气候变化的敏感性，除构造沉降外，气候因素也是控制层序发育以及湖盆中烃源岩形成的尤为重要的因素。

But in lacustrine basins , the sedimentary process is very sensitive to climatic changes , the climate is also a very important factor controlling the sequence development and hydrocarbon source rock formation in lacustrine basins .

河西走廊东段湖泊旋回及其古气候意义

Lake Cycle and Its Paleoclimatic Significance in Eastern Hexi Corridor

中昆仑山区封闭湖泊湖面波动及其气候意义

Fluctuation of closed lake-level and its climatic significance on the middle Kunlun Mountains

西北地区近年来内陆湖泊变化反映的气候问题

Climate Change Indicated by the Recent Change of Inland Lakes in Northwest China

中国西部湖泊水量对未来气候变化的响应&蒙特卡罗概率法在气候模拟输出的应用

Preliminary Study on the Responses of Lake Water from the Western China to Climate change in the Future : Monte Carlo Analysis Applied in GCM Simulations and Lake Water Changes

具有环境敏感性指针的低海拔沙化和高海拔湖泊变化与区域气候变化呈高度耦合性，反映环境变化在水平和垂直空间尺度的协同性。

Desertification at relative low altitude and lakes at relative high altitude simultaneously changed which was highly consistent with the regional climate change ; all of this shows that environmental change in the horizontal and vertical spatial scales is consistent .

在湖泊沉积的古气候研究中，沉积物粒度的气候指示意义常被解释为，粗粒沉积物指示低水位时期的干旱气候，而细粒沉积物则反映高水位时期的湿润气候。

In the research of paleoclimate of lacustrine sediments , the grain size is of climatic significance . The coarse sediments reflect arid climate characterized by low-water period , while , fine sediments indicate humid climate characterized by high-water period .

湖泊沉积物真实地记载了湖泊过去气候、环境变迁的信息，人类活动对湖泊环境的影响也保存在该地质记录中，因此湖泊沉积物包括了气候变化和人类活动的双重影响。

Sediments record the past climate , environmental change and the influence imposed by human being in lake in truth , which include double effects of climatic change and human being 's activities .

湖泊自生碳酸盐碳氧同位素变化是反映内陆湖泊水环境与气候环境的重要指标。

Authigenic carbonate oxygen and carbon isotope evidence in lake sediment is an important proxy to reflect lake environment and climatic change .

区域湖泊综合对比结果进一步表明，不同湖泊盐度和水文变化趋势一致，反映了封闭湖泊对区域气候变化的共同响应特点。

The consistency between the lake salinity and hydrological changes by regional comparison reveals that the common response of these inland lakes to regional climate changes further supports our conclusion .